Results 41 to 50 of about 43,336 (208)

Multiproxy tree ring reconstruction of glacier mass balance: insights from Pinus cembra trees growing near Silvretta Glacier (Swiss Alps) [PDF]

open access: yesClimate of the Past
Glacier mass balance reconstructions provide a means of placing relatively short observational records into a longer-term context. Here, we use multiple proxies from Pinus cembra trees from God da Tamangur, combining tree ring anatomy and stable isotope ...
J. Lopez-Saez   +12 more
doaj   +1 more source

Mass-balance modelling of Gangotri glacier

open access: yesGeological Society, London, Special Publications, 2017
Abstract The sensitivity of glacier mass balance (MB) in response to climatic perturbations has made it an important parameter of study from hydrological, climatological and glaciological point of view. To monitor the health of any glacier system, long-term MB observations are required. These observations among Himalayan glaciers
A. Agrawal, R.J. Thayyen, A.P. Dimri
openaire   +1 more source

Heterogeneous glacier thinning patterns over the last 40 years in Langtang Himal [PDF]

open access: yes, 2016
Himalayan glaciers are losing mass at rates similar to glaciers elsewhere, but heavily debris-covered glaciers are receding less than debris-free glaciers or even have stable fronts.
Bolch, Tobias   +2 more
core   +1 more source

Temporal downscaling of glaciological mass balance using seasonal observations

open access: yesJournal of Glaciology, 2023
Glaciological mass-balance measurements have been the backbone of internationally coordinated glacier monitoring. The resulting annual observations have been used to understand glacier reactions to climate change, and to assess both regional and global ...
Michael Zemp, Ethan Welty
doaj   +1 more source

Global glacier mass balance and mass balance partitioning from radar altimetry

open access: yes, 2023
The 28th IUGG General Assembly (IUGG2023) (Berlin 2023)
Gourmelen, N., Livia, J.
openaire   +2 more sources

One Decade of Glacier Mass Changes on the Tibetan Plateau Derived from Multisensoral Remote Sensing Data [PDF]

open access: yes, 2014
The Tibetan Plateau (TP) with an average altitude of 4,500 meters above sea level is characterized by many glaciers and ice caps. Glaciers are a natural indicator for climate variability in this high mountain environment where meteorological stations are
Neckel, Niklas
core   +1 more source

Sensitivity of mountain glacier mass balance to changes in bare-ice albedo

open access: yesAnnals of Glaciology, 2017
Albedo is an important parameter in the energy balance of bare-ice surfaces and modulates glacier melt rates. The prolongation of the ablation period enforces the albedo feedback and highlights the need for profound knowledge on impacts of bare-ice ...
Kathrin Naegeli, Matthias Huss
doaj   +1 more source

Annual mass-balance time series of Dongkemadi Glacier, 2000–20, from a linear albedo-based model using geodetic data and validated with the glaciological method

open access: yesJournal of Glaciology
Long-term time series of annual glacier mass balance is important for revealing a glacier's response to regional climate variations. However, for the Tibetan Plateau, time series of annual glacier mass balance with more than 10 consecutive years remains ...
Lin Liu   +4 more
doaj   +1 more source

Extrapolating glacier mass balance to the mountain-range scale: the European Alps 1900–2100 [PDF]

open access: yesThe Cryosphere, 2012
This study addresses the extrapolation of in-situ glacier mass balance measurements to the mountain-range scale and aims at deriving time series of area-averaged mass balance and ice volume change for all glaciers in the European Alps for the period 1900–
M. Huss
doaj   +1 more source

Mass-balance characteristics of arctic glaciers [PDF]

open access: yesAnnals of Glaciology, 2005
AbstractA survey of available mass-balance data shows that glaciers on arctic islands, i.e. mountain glaciers and ice caps in northern Canada, Greenland, Svalbard and the Eurasian islands, share mass-balance characteristics of low annual amplitude and small interannual variability. By contrast, glaciers around the Arctic (e.g.
openaire   +1 more source

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